Soil scientists Brian Wienhold (left) and Gary Varvel compare corncob residue in various stages of decomposition in a no-till field in Lincoln, Nebraska. In this study and several others, ARS researchers were surprised to learn how much carbon corn and switchgrass sequester in the soil between 12 inches and 5 feet deep. Photo by Peggy Greb.

This story comes to us from USDA ARS’s Ag Research Journal, authored by Ann Perry. After reading it, Rachel and Kathy got on the phone to talk about how exciting this information is. First, it calls into question things we thought we knew about soil carbon and where it was in the soil profile. It also represents a kind of science that’s hard to do. You need special equipment and sampling techniques that go beyond the usual ‘send a grad student into the field with a shovel and a bucket’ and can’t be funded by a more-typical inexpensive grant. Finally, understanding where carbon is stored and how we might improve that process means that farmers and ranchers can be superheroes when it comes to cooling the planet. Since each of the last 3 years have each been labeled the hottest on record, this could be a big deal! You go, Superheroes!

For years, many agronomists believed that significant levels of soil carbon only accumulated near the soil surface. So when four Agricultural Research Service scientists submitted a research paper claiming that large amounts of soil carbon were sequestered as deeply as 5 feet in the soil profile—and by annual as well as perennial crops—they had some trouble getting their paper through the review process.

The study was a 9-year project that evaluated the effects of nitrogen fertilizer and harvest treatments on soil organic carbon sequestration in switchgrass and no-till maize crops managed for biofeedstock production.

“Soil organic carbon sequestration has a major impact on the long-term sustainability of bioenergy crop production because it can significantly affect soil fertility and greenhouse gas emissions,” says ARS geneticist Ken Vogel (retired). “So using accurate sequestration rates is essential in developing life-cycle analyses that assess the long-term environmental costs and benefits of biofuel crop production.” [Editors note: That’s why they started the research, and why they looked at the crops they looked at. But keep in mind that the results help us understand what’s going on under the soil in other areas as well.]

Vogel, soil scientists Ron Follett (retired) and Gary Varvel, and agronomist Rob Mitchell conducted their study on marginally productive fields similar to the croplands that would be suitable for commercial switchgrass production. Mitchell and Varvel are with ARS research units in Lincoln, Nebraska. Follett was with ARS in Fort Collins, Colorado.

The team established large plots that could accommodate field-scale equipment and took baseline soil samples to a depth of 5 feet before the first crops were cultivated. These baseline samples showed that soil organic carbon levels varied within the first foot of the subsoil by as much as around 18 tons per acre, while soil carbon levels 5 feet below the soil surface varied by as much as almost 90 tons per acre.

Soil Carbon Stores: Annual vs. Perennial

Soil scientist Ron Follett (right) examines a map of ARS soil carbon research sites across the United States while physical science technician Ed Buenger conducts mass spectrophotometer analysis of soil samples for carbon and nitrogen. Photo by Stephen Ausmus.

To explore this phenomenon, the scientists then planted two switchgrass cultivars and no-till maize and applied nitrogen fertilizers at three different rates ranging from 54 pounds per acre to around 160 pounds per acre. Nitrogen fertilizers support biomass production, and the scientists wanted to see if the production of more plant biomass resulted in sequestration of more carbon in the soil. Some switchgrass plots were also maintained without any nitrogen amendments.

Postharvest crop residue, or “stover”—which also contributes to soil carbon—was not removed on half of the no-till maize fields; on other fields, half of the stover was removed. After the crops were established, the researchers resampled soils in the production fields at 3-year intervals.

What was their biggest surprise? In the no-till maize field, soil organic carbon levels increased over time at all depths, with all nitrogen treatments, and with either type of postharvest stover management. Almost all increases were statistically significant. Maize grain yields were greatest from fields that had been amended with 107 pounds of nitrogen per acre and where no stover had been removed, a management strategy that resulted in an average annual increase in soil carbon that exceeded 0.9 tons per acre.

The researchers were equally surprised that more than 50 percent of the soil organic carbon was found at depths between 1 foot and 5 feet below the soil surface. This region of the soil profile, which typically has not been sampled by other researchers investigating carbon sequestration levels, is below the tillage zone and is therefore more stable over time.

In the switchgrass plots, the researchers also observed impressive increases of soil carbon sequestration throughout the soil profile. Sequestration rates increased as nitrogen fertilization rates increased, and almost all increases of soil carbon were statistically significant.

As they observed with the no-till maize plots, more than 50 percent of the soil carbon was found between 1 and 5 feet below the soil surface. The average annual increase of soil organic carbon throughout the first 5 feet of subsoil also exceeded 0.9 tons per acre per year, which was equivalent to 3.25 tons of carbon dioxide per acre per year.

“We had not expected to find these stores of deep soil carbon, even though we always knew plant roots reached this deep, because we didn’t realize how much the activity around roots can affect soil carbon budgets,” Follett says. “Most studies only sample soils for carbon to a depth of 18 inches.”

Because of their findings, the team concluded that calculating soil carbon sequestration rates for bioenergy crops is not a one-size-fits-all proposition. Crop selection, soil differences, environmental conditions, and management practices affect sequestration rates differently from one region to another. As a result, bioenergy crop production models will probably need some major adjustments.

“Our work suggests that carbon sequestration rates used in current life-cycle analysis models for bioenergy crops are probably resulting in underestimates of how much carbon is being sequestered in the soil,” says Vogel. “It also highlights how nitrogen amendments and other management decisions do matter when it comes to corn and carbon sequestration—and that annual crops can make important contributions to soil carbon.”

The paper was accepted by Bioenergy Research and published in 2012. But even though its results were so surprising, two other ARS studies had highlighted similar dynamics

In 2011, results from a related long-term soil carbon study conducted by Varvel and his ARS colleague Wally Wilhelm (deceased) were published in Soil & Tillage Research. The researchers had studied soil carbon levels in fields established in 1980 for three different nonirrigated cropping systems—continuous corn, continuous soybean, and a soybean/corn rotation—that were managed with six different tillage systems.

In 1999, as part of the study, Varvel and Wilhelm collected soil samples from these fields at several intervals to a depth of 5 feet. They found that tillage management and crop selection independently affected soil nitrogen and carbon levels and that the highest levels of nitrogen and carbon had accumulated in the continuous-corn cropping system under no-till management. But as with the later study, the biggest surprise was how much nitrogen and carbon accumulated in the soil profile between 12 inches and 5 feet in all the cropping and tillage systems.

“When we collected these samples, many soil scientists believed that annual field crops don’t sequester carbon in conventional tillage systems, so the results were a shock,” says Varvel. “But conducting a long-term study allowed us to observe what happens with soil carbon sequestration once a management system is established and the year-to-year variations diminish.” He also noted that identifying these deeper pools of carbon and nitrogen can help growers more effectively select tillage management that helps retain these nutrients in the soil.

These findings aligned with results from an 8-year study, published in 2013, that Follett conducted on carbon sequestration in no-till and conventional-till irrigated continuous corn systems near Fort Collins. He and Fort Collins soil scientist Ardell Halvorson found that no-till management resulted in higher levels of soil carbon than did conventional tillage and that those levels didn’t change much over the 8 years.

The team measured carbon levels in the soil to a depth of 4 feet and found that the amount of longstanding soil carbon lost after conventional tillage was greater than the amount of carbon added to the soil from stover biomass. These results highlighted the need to learn more about older soil carbon pools deep in the soil profile and whether these carbon levels decline as a result of soil microbial activity, irrigation, or other processes.

“Some of the soil carbon in these soils is thousands of years old and is very stable, so its disappearance was a surprise,” says Follett, who published the results in Soil Science Society of America Journal. “Regular irrigation of the typically semiarid soil could be one of the factors that resulted in the carbon loss, but we would need to conduct additional studies to determine that.”

Follett notes that the soil microbial groups in these environments still need to be identified, as do the environmental shifts that allow these microbes to more easily access the carbon for their own use. He also shares Varvel’s belief that these findings underscore how farmers can use no-till management to conserve soil carbon deep in the soil profile—and the value of long-term studies for understanding soil carbon dynamics.

“It takes time for new management systems to have any effect on soil carbon. Identifying these effects can require long-term studies, sampling deeper within the soil profile, and using advanced measurement techniques,” Follett says. “We’re looking for little changes in a great big pool.”

This research is part of Pasture, Forage, and Rangeland Systems (#215), Bioenergy (#213), and Climate Change, Soils, and Emissions (#212), three ARS national programs described at www.nps.ars.usda.gov. To reach scientists mentioned in this article, contact Ann Perry, USDA-ARS Information Staff, 5601 Sunnyside Ave., Beltsville, MD 20705-5128; (301) 504-1628.

“A Surprising Supply of Deep Soil Carbon” was published in the February 2014 issue of Agricultural Research magazine.

About the author

Kathy worked with the Bureau of Land Management for 12 years before founding Livestock for Landscapes in 2004. Her twelve years at the agency allowed her to pursue her goal of helping communities find ways to live profitably AND sustainably in their environment. She has been researching and working with livestock as a land management tool for over a decade. When she's not helping farmers, ranchers and land managers on-site, she writes articles, and books, and edits videos to help others turn their livestock into landscape managers.

4 Comments

I am so pleased to have the article ON PASTURE sent to me. I started totally Organic Farming on my 32 cow dairy farm in 1953. This was after my bad experience with 24-D herbicide in 1949. Never used it again. This prompted me to experiment for three years testing organic vs chemicals. My 32 cow dairy herd taught me they wanted organic over chemically grown pasture and roughage. They are the best chemists if given a choose and they took organic every time. I will send you a book — Learned by the Fencepost– I had published in 2011. I also wish you would type on Google ALADAY LLC Is Monsanto a Monster a post that was chosen as a guest wrier. Please get back in touch we can learn allot from each other

This article On Pasture made my day. I started Organic Farming on my 32 cow dairy farm in Vermont in 1950. The use of 24-D herbicide in 1949 started me to experiment with Organic in 1950. I used to much herbicide at turn around and left a quarter moon circle where nothing grew for years. My three years of experiments 1950 thru 1952 proved to me Organic was superior to chemicals. My cows with their four stomach were my teachers. Also the earthworms as well. I stopped use all chemicals in 1953. I 1958 I won the New England Green Pasture contest over thousands of chemical Farmers. I never took any grant money as I did not want money interfering with my common sense and logic. My theme is FERTILE SOIL IS THE LIFE BLOOD OF THE EARTH AND ALL FOOD COMES FROM THE SOIL — FOOD — HEALTH IN THIS ORDER. It was before the hot acid chemicals have turned the organic matter (carbon) to CO2 the green house gas causing global warming. What did not go to the atmosphere has leached to the water ways causing unbelievable fish kill.
Please type on Google ALADAY LLC Is Monsanto a Monster it is an article I wrote as a guest writer. Thank you get back in touch.

To Edmund: Corn after corn cannot build enough soil carbon unless one uses the organic method to feed the plants. Chemical fertilizer hot acids burn up the SOM and overload the plants intake of nitrogen. The soil carbon is now CO2 the green house gas causing global warming. There is no root system as not needed.

The big mistake that organic people make is the soil has to be prepared differently than for chemicals. There is 78% N in the atmosphere that can be trapped with deep till and organic matter when it rains. This is the same with oxygen 20% that hardly is mentioned but necessary for the earthworms and microoganisims. Both elements are gas and will disspatate back to the atmosphere if not held. it takes time to get the soil back if chemicals have been used before. The rototillers do not go deep enough buy just cause a shallow hardpan that organic roots cannot penetrate.